Understanding gold-(silver)-telluride-(selenide) mineral deposits

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2009-12-01
Authors
Cook, Nigel
Ciobanu, Cristiana
Spry, Paul
Voudouris, Panagiotis
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Spry, Paul
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Geological and Atmospheric Sciences

The Department of Geological and Atmospheric Sciences offers majors in three areas: Geology (traditional, environmental, or hydrogeology, for work as a surveyor or in mineral exploration), Meteorology (studies in global atmosphere, weather technology, and modeling for work as a meteorologist), and Earth Sciences (interdisciplinary mixture of geology, meteorology, and other natural sciences, with option of teacher-licensure).

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The Department of Geology and Mining was founded in 1898. In 1902 its name changed to the Department of Geology. In 1965 its name changed to the Department of Earth Science. In 1977 its name changed to the Department of Earth Sciences. In 1989 its name changed to the Department of Geological and Atmospheric Sciences.

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1898-present

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  • Department of Geology and Mining (1898-1902)
  • Department of Geology (1902-1965)
  • Department of Earth Science (1965-1977)
  • Department of Earth Sciences (1977-1989)

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Abstract

Gold-(silver)-telluride (selenide) ores occur as epithermal orogenic and intrusion related deposits. Although Te and Se are chalcophile elements and share geochemical affinity with Au, formation of selenides and other elements Ag-Au require acidic or reducing environments. The thermodynamic stability conditions for Au and Agtellurides and native tellurium indicate an epithermal environment. Analysis of mineral paragenensis, textures and compositional variation in tellurides/selenides suggest petrogenetic processes involving interaction with fluids leading to Au scavenging and entrapment in tellurides, changes in chemistry/rates of fluid infiltration and attaining equilibrium in a given assemblage.

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This article is published as Cook, Nigel J., Cristiana L. Ciobanu, Paul G. Spry, and Panagiotis Voudouris. "Understanding gold-(silver)-telluride-(selenide) mineral deposits." Episodes Journal of International Geoscience 32, no. 4 (2009): 249-263. doi:10.18814/epiiugs/2009/v32i4/002.

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Thu Jan 01 00:00:00 UTC 2009
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